Crater of Diamonds State Park facts for kids
Quick facts for kids Crater of Diamonds State Park |
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![]() Digging for diamonds, 2007
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Location | Murfreesboro, Pike, Ouachita Mountains, Arkansas, United States |
Area | 911 acres (369 ha) |
Established | 1972 |
Named for | Diamond mine |
Governing body | Arkansas Department of Parks and Tourism |
Website | Crater of Diamonds State Park |
Crater of Diamonds State Park is a special state park in Pike County, Arkansas, in the United States. It covers about 911 acres (369 hectares). The park is famous for its 37.5-acre (15.2 ha) plowed field. This field is the only place in the world where you can dig for diamonds and keep what you find!
People have been finding diamonds here since 1906. One famous diamond found was the Strawn-Wagner Diamond. The area became a state park in 1972. This happened after the Arkansas Department of Parks and Tourism bought the land. Before that, different companies ran it as a place for tourists to visit.
Contents
History of Diamond Discoveries
In August 1906, a farmer named John Huddleston found two unusual crystals on his farm near Murfreesboro, Arkansas. The next month, John and his wife, Sarah, sold the rights to their farm to some investors from Little Rock. These investors wanted to see if the land truly had diamonds.
After 1906, people tried to mine diamonds on a large scale. But these attempts usually failed. Most of the diamonds found came from the top layer of soil. Over a long time, rain and wind had washed diamonds into this layer. In the early days (1907–1932), many diamonds were found in this "black gumbo" surface.
Old mining equipment often missed smaller diamonds. These tiny gems ended up in the park's drainage areas. Today, these small diamonds are what many visitors find when they dig.
The Diamond Rush and Boomtowns
When the first diamond was found, it caused a "diamond rush" in the area. Murfreesboro became a very busy "boomtown." Stories say that hotels in Murfreesboro turned away thousands of people. These hopeful diamond miners supposedly set up a tent city nearby. They called it "Kimberly," after the famous diamond area in South Africa.
However, records show that the town of Kimberly was actually a land project started in 1909. It was meant to be a new town, but the diamond excitement faded, and the project failed. Today, the Kimberly area is mostly farmland.
From Private Mine to State Park
During World War II, the U.S. government took over the mine. They wanted to get diamonds for the war effort. Diamonds were found, but it was very expensive to mine them with U.S. workers. After the war, the land went back to its previous owners.
From 1951 to 1972, different private companies ran the diamond site as a tourist spot. Howard A. Millar and his wife, Modean, opened their "Crater of Diamonds" attraction in 1952. Howard was a good writer and helped make the park famous. In 1956, a visitor found the Star of Arkansas, a beautiful 15.33-carat diamond.
Later, another tourist attraction opened nearby. This competition made both businesses weaker. In 1970, a company called General Earth Minerals (GEM) bought all the land. They later sold it to the State of Arkansas in March 1972 for $750,000. That's when it officially became Crater of Diamonds State Park.
Because of this park, and because Arkansas was the first place outside South Africa where diamonds were found in their original source, diamonds became a symbol for the state. A large diamond symbol has been on the state flag since 1912. Also, the Arkansas State Quarter, made in 2003, has a diamond on it.
Geology of the Diamond Crater
The Crater of Diamonds is part of an old, eroded volcano that is about 95 million years old. Deep inside the Earth, hot liquid rock called magma brought the diamonds to the surface. These diamonds formed very, very deep in the Earth's upper mantle. They were picked up by the magma as it traveled upwards.
Geologists have studied this area to understand how the diamonds formed. One geologist, Roland Everett Langford, wrote about it in 1973. Later, another geologist, Dennis Dunn, did more research in 2002. He found that the diamonds came from a special type of rock called lamproite.
Most diamonds around the world come from a different type of rock called kimberlite. But the Crater of Diamonds is special because its diamonds come from lamproite. The Argyle diamond mine in Australia is another famous lamproite diamond source.
Fun Activities at the Park
Crater of Diamonds State Park is famous for its 37.5-acre (15.2 ha) plowed field. Here, visitors can hunt for diamonds and other cool gems. On average, park visitors find about two diamonds every day!
The park has a visitor center where you can learn about the park's geology. There's also a gift shop and a cafe. You can also visit the Diamond Discovery Center. It teaches you how to look for diamonds. The park also has a water play area called Diamond Springs. There are also picnic spots and trails to explore. If you like camping, the park has 47 camping spots near the Little Missouri River.
The Diamond Search Field
The park is built over an old volcanic pipe made of lamproite rock. For a small fee, visitors can dig for diamonds and other gemstones. People who love to search for rocks are called rockhounds.
Park visitors find over 600 diamonds every year! These diamonds come in all sorts of colors and types. More than 29,000 diamonds have been found since it became a state park. The best part? You get to keep any gemstone you find, no matter how valuable it is!
Besides diamonds, you might find other cool gems. These include amethyst, agate, and jasper. You might also find about 40 other minerals like garnet, quartz, and calcite.
Famous Diamonds Found Here
Year | Finder | Diamond Name | Weight (carat) | Weight (gram) | Color | Notes |
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1917 | Lee J. Wagner | 17.86 | 3.572 | canary yellow | on display in the National Museum of Natural History | |
1924 | Wesley Oley Basham | Uncle Sam | 40.23 | 8.046 | largest diamond ever discovered in the United States | |
1964 | John Pollock | Star of Murfreesboro | 34.25 | 6.850 | ||
1975 | W. W. Johnson | Amarillo Starlight | 16.37 | 3.274 | Largest found since 1972. Cut into a 7.54-carat marquise shape. | |
1977 | George Stepp | Kahn Canary | 4.25 | 0.850 | canary yellow | Naturally perfect. It's still in its original "pillow" shape. |
1978 | Betty Lamle | Lamle Diamond | 8.61 | 1.722 | fourth largest found since 1972 | |
1981 | Carroll Blankenship | Star of Shreveport | 8.82 | 1.764 | second largest found since 1972 | |
1990 | Shirley Strawn | Strawn-Wagner Diamond | 3.09 | 0.618 | cut to 1.09 carats in 1997. It was graded "perfect" in 1998. You can see it at the park. | |
1991 | Joe Fedzora | Bleeding Heart Diamond | 6.23 | 1.246 | brownish yellow | |
1997 | Richard Cooper | Cooper Diamond | 6.72 | 1.344 | deep purplish-brown | |
1997 | Richard Cooper | Cooper Diamond | 6.00 | 1.200 | brown/cognac | New owners from Florida since 2008. |
2006 | Marvin Culver | Okie Dokie Diamond | 4.21 | 0.842 | deep canary yellow | Perfect. Featured on TV shows and in magazines. |
2006 | Bob Wehle | Sunshine Diamond | 5.47 | 1.094 | deep canary yellow | Perfect. |
2006 | Donald and Brenda Roden | Roden Diamond | 6.35 | 1.270 | honey brown | |
2007 | Chad Johnson | 4.38 | 0.876 | tea-colored | ||
2008 | Denis Tyrrell | Kimberly Diamond | 4.42 | 0.884 | ||
2008 | Richard Burke | Sweet Caroline | 4.68 | 0.936 | white | |
2009 | Glenn Worthington | Easter Sunrise Diamond | 2.04 | 0.408 | yellow | |
2010 | Glenn Worthington | Brown Rice Diamond | 2.13 | 0.426 | light brown | |
2011 | Beth Gilbertson | Illusion Diamond | 8.66 | 1.732 | white | third largest diamond found since 1972, and largest in almost 30 years |
2013 | Michael Detlaff | God’s Glory Diamond | 5.16 | 1.032 | honey brown | |
2013 | Tana Clymer | God's Jewel | 3.85 | 0.770 | canary yellow | |
2014 | Brandon Kalenda | Jax Diamond | 2.89 | 0.578 | white | |
2014 | David Anderson | Limitless Diamond | 6.19 | 1.238 | white | |
2015 | Susie Clark | Hallelujah Diamond | 3.69 | 0.738 | white | |
2015 | Bobbie Oskarson | Esperanza Diamond | 8.52 | 1.704 | Type IIa, D IF | The fifth largest diamond found since 1972. It was cut and polished in Arkansas by a master diamond cutter. |
2017 | Kalel Langford | Superman's Diamond | 7.44 | 1.488 | dark brown | |
2019 | Josh Lanik | Lanik Family Diamond | 2.12 | 0.424 | dark brown | |
2019 | Miranda Hollingshead | Caro Avenger | 3.72 | 0.744 | light yellow | |
2020 | Kevin Kinard | Kinard Friendship Diamond | 9.07 | 1.814 | brandy brown |